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Petrology of the Kurançalı ultramafic-mafic cumulates characterized by hydrous phases (central Turkey): crystallochemical implications
Date
2005-10-04
Author
Toksoy Köksal, Fatma
Oberhänsli, Roland
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https://hdl.handle.net/11511/72317
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Petrology of the phlogopite-bearing ultramafic-mafic plutonic rocks within Central Anatolian crystalline complex, Turkey
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Petrology of the Kurancali phlogopitic metagabbro: An island arc-type ophiolitic sliver in the Central Anatolian Crystalline Complex
Toksoy-Köksal, Fatma; Göncüoğlu, Mehmet Cemal; Yalınız, Mustafa Kenan (2001-07-01)
The Kurancali metagabbro occurs as an isolated body in the central part of the Central Anatolian Crystalline Complex. It has been emplaced along a steep S-vergent thrust-plane onto the uppermost units of the Central Anatolian Metamorphics. The main body of the Kurancali metagabbro is characterized by distinct compositional layering. The layered gabbros comprise pyroxene and hornblende gabbros. Phlogopite-rich, plagioclase-hornblende gabbro occurs mainly as pegmatitic dikes intruding the layered gabbro seque...
Petrological Characteristics and LA SF ICP MS U Pb ages of S type Granitoids from Central Turkey
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Petrology geochemistry and mineralogy of Orhaneli ultramafic rocks and associated chromite deposits.
Tankut, Ayla; Proctor, P. D.; Tokay, M.; Department of Geological Engineering (1977)
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F. Toksoy Köksal and R. Oberhänsli, “Petrology of the Kurançalı ultramafic-mafic cumulates characterized by hydrous phases (central Turkey): crystallochemical implications,” 2005, Accessed: 00, 2021. [Online]. Available: https://hdl.handle.net/11511/72317.
